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A simultaneous increase in the cosmogenic nuclides Be suggests that these changes in climate and vegetation were forced by a sudden decline in solar activity.

Expansion of pine occurred during the later part of the Late Preboreal.

The Dutch records show that following the Lateglacial/Holocene climate warming, birch woodlands expanded between 11,530 and 11,500 cal BP during the Friesland Phase of the Preboreal.

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Detailed multi-proxy analyses including microfossils (e.g., pollen, spores, algae, and fungal spores), macroremains (e.g., seeds, fruits, wood, mosses, etc.), and loss on ignition measurements were carried out with high temporal resolution.

To link the five Preboreal records, accurate chronologies were produced by AMS C wiggle-match dating.

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